Indonesia earthquake: Torrents of 'liquid soil' washed away buildings
CNN/Stylemagazine.com Newswire | 10/3/2018, 5 a.m.
By Bard Wilkinson, CNN
(CNN) -- Rivers of soil swept away entire neighborhoods in Indonesia following a powerful earthquake last week that also generated a tsunami in a disaster that has killed at least 1,407 people.
Experts say the destruction is due to soil liquefaction, a process occurring when soil becomes saturated with water causing it to erupt into tumultuous torrents, as it did on Friday, shifting and tumbling buildings.
Footage has emerged from the stricken city of Palu showing people running to find solid ground as structures were swept away and destroyed by waves of undulating earth. Images show a section of the city being erased by surging soil.
In Petobo town the ground under the length of an entire main road was torn up, with the tide of soil leaving broken stretches of tarmac-topped debris in wave-shaped mounds and troughs.
"Liquefaction occurs when loose sandy soils with shallow groundwater are subjected to sudden loading such as shaking from an earthquake," said Jonathan Stewart, professor of Civil and Environmental Engineering Department at UCLA.
Many experts liken the process to waves lapping on a sandy beach. When the waves come in, the sand softens, but when the waves withdraw, the sand stiffens.
"During the earthquake, water pressure is generated in the soil, which causes a dramatic loss of strength," said Stewart. "The strength loss can be so great that the soil behaves almost like a liquid."
Soil running downhill, known as "flow failure," is one of the most severe effects of liquefaction, and prone to occur in areas with a particular soil structure.
"The soils in the slide area are likely geologically young, loose, sandy materials with shallow groundwater," said Stewart.
Was the earthquake triggered by a volcano?
Scientists say that the devastating sequence of natural disasters were the result of a highly unusual series of geological events, which may be related to the eruption on Wednesday of the Soputan volcano, also on Sulawesi island.
"Did the bulging magma chamber of the volcano trigger the earthquake? Or did the earthquake trigger the magma chamber to pass magma to the funnel of the volcano?" said Professor Costas Synolakis, director of the University of South California Tsunami Research Center.
According to Synokalis, volcanic eruptions are very often preceded by swarms of earthquakes, which are typically smaller than magnitude 5.
"It is all beginning to look like a Hollywood movie scenario," added Synokalis. "A (7.5 magnitude) earthquake with a mechanism not usually associated with tsunamis triggers a big one, and volcanic activity at a distance from the earthquake far larger than usually expected for causation."
The epicenter of Friday's earthquake was on land and not at sea, meaning the probability of a tsunami was low. Many experts have theorized that the tsunami was therefore triggered not by the earthquake itself but by a submarine landslide caused by the earthquake.
Though such a chain of events are rare and therefore difficult to mitigate, scientists say that engineering techniques do exist to lessen the impact of soil liquefaction.